Sm-Nd isotopic compositions of Cambrian-Ordovician strata at the Jinggangshan area in Jiangxi Province: Tectonic implications

Whole-rock Sm-Nd isotopes were investigated for Cambrian-Ordovician strata from the Jinggangshan area between the Yangtze Block and Cathysia Block in South China. These strata were deposited as a greatly thick unit of muddy-sandy laminas with intercalated carbonate and organic carbon-bearing layers. They have low εNd（t） values of -13.9 to -7.9 and old Nd model ages of 1842 to 2375 Ma. In tDM-tStr diagram, they are far away from the concordant line but fall within the evolution zone of the Proterozoic crust of South China. This indicates that the Cambrian-Ordovician strata are mainly composed of matters eroded from ancient Paleoproterozoic crust that may mainly consist of continental-derived detrital sediments with high maturity in the Cathysia Block. However, the Ordovician Jueshangou Formation and Dui＇ershi Formation have εNd（t） values of -10.5 and -7.9 at the higher end of the above range and Nd model ages of 1842 to 2059 Ma at the lower end of the above range. This suggests involvement of more detritus that were eroded from the relatively juvenile crust from Late Paleoproterozoic to the Early Neoproterozoic. All the Nd model ages for the Cambrian-Ordovician sedimentary rocks in the Cathysia Block and the southeastern margin of the Yangtze Block are older than 1800 Ma, suggesting that no material from the Early Paleozoic depleted mantle-derived magmas was involved in these regions.     

A Chengjiang-type fossil assemblage from the Hongjingshao Formation （Cambrian Stage 3） at Chenggong,Kunming, Yunnan

A new Chengjiang-type fossil assemblage is reported herein from the lower part of the Hongjingshao Formation at Xiazhuang village of Chenggong,Kunming,Yunnan.The fossil assemblage,named as Xiazhuang fossil assemblage,yields predominantly soft-bodied fossils,including arthropods,brachiopods,priapulids,lobopods and some problematic taxa,with arthropods being the most dominant group.Preservation and composition of the fossil assemblage are very similar to the typical Chengjiang biota,which is preserved in the middle Yu’anshan Formation in the large area of eastern Yunnan.The associated trilobites demonstrate that the soft-bodied fossil assemblage belongs to the late Qiongzhusian in age(Stage 3,Cambrian),suggesting that the Hongjingshao Formation is probably a diachronous lithostratigraphic unit ranging from the upper Qiongzhusian to the lower Canglangpuan stages in eastern Yunnan.The fossil assemblage from the Xiazhuang area fills up the missing link between the typical older Chengjiang biota and the younger Malong and Guanshan biotas,making eastern Yunnan a unique area in the world to reveal the early evolutionary history of animals and palaeocommunity dynamics during the‘‘Cambrian explosion’’.     

湘鄂—江南隆起区寒武系黑色页岩有机地球化学特征

我国南方页岩气藏发育的最有利区位于四川盆地、米仓山—大巴山前陆以及渝东、黔北、湘鄂—江南隆起北缘一线,寒武系地层普遍发育黑色泥页岩,这套黑色泥页岩是早寒武世早期全球性海平面上升时,在区域性深水滞留缺氧的陆棚到斜坡环境沉积的,具有单层厚度大、发育层位多、分布面积广、热演化程度高、后期改造强等特点,构成了中国南方页岩气发育的强大物质基础。以黑色碳质泥质岩类为重点,对其有机碳丰度、可溶沥青丰度与组成、干酪根特征等方面进行了较为系统的有机地球化学分析;结合有机质演化阶段,为页岩气藏的远景评价和地质勘探工作提供参考。     

页岩气成藏体系研究——以四川盆地及其周缘下寒武统为例

页岩气是非常规天然气藏的一种,属于"单源一位"成藏体系,在成藏特征上不同于常规油气,集烃源体、输导体和圈闭体等所有关键的成藏体系各要素于同一套页岩层.在成藏体系的划分上,页岩气藏不同于常规成藏体系的划分.综合考虑页岩层系发育时代、沉积特征、演化历史、所处现今大地构造位置、构造特征、页岩残留状况、分布特点、埋深和含气量等因素,提出了页岩气成藏体系划分的一般性原则.将四川盆地及其周缘下寒武统页岩气成藏体系划分为川南—川东南、黔北—黔中、渝东、湘鄂西、龙门山、米仓山—大巴山和川中7个成藏体系,并按战略展开区、战略突破区、战略准备区和战略远景区4个层次对成藏体系进行了评价,明确了勘探层次.     

辽宁晚寒武世一些原始真牙形石的组织学研究

采用油浸法对辽宁本溪及复县晚寒武世的一些真牙形石分子的组织进行了研究.共对6个原始真牙形石种Proconodontus muelleri,Proconodontus tenuiserratus,Granatodontus ani,Rotundoconus tricarinatus,Teridontus nakamurai和Cordylodus Proavus的组织学特征进行了详细的描述.在最原始的真牙形石种Proconodontus tenuiserratus基体中发现了管状牙本质;在Proconodontus muelleri基体中识别出平行的层状组织、波层状组织;此外,分别在真牙形石种Granatodontus ani和Rotundoconus tricarinatus的基体中发现了管状牙本质和球状牙本质.发现Miller(Univ Kansas Paleontol Contr,1980,99:1-39)提出的Proconodontus谱系和Teridontus谱系的牙形石的组织特征基本相同.因而提出,真牙形石很有可能是单系起源的.     

塔东地区寒武系—下奥陶统成岩作用特征及对优质储层形成的影响

通过对塔东地区寒武系-下奥陶统7口井岩心观察及薄片分析鉴定,发现寒武系-下奥陶统成岩演化过程复杂,各种成岩作用发育.对储层形成有建设性作用的有白云石化、溶蚀、破裂作用; 具破坏性的成岩作用有黄铁矿化、硅化、压实和充填作用等.以白云石岩石学特征为基础,结合构造背景,认为研究区广泛发育的白云岩为构造热液白云石化成因,断裂系统为热液白云石化提供了热源流体.随着成岩作用演化的加深,岩层演化的总趋势是越来越致密,最终使孔隙度偏低,储层性能较差;但经过热液白云石化成岩演化过程比未经过此过程的岩石具有较高的孔隙度,更有利于储层的发育.     

穿越生命之痛的美

<正>28岁时,金星把自己的身份由"他"变成了"她",这是一次凤凰涅槃的重生。她不是传统意义上的完美女人,但却拥有独立的个性。她的人生太曲折、经历太离奇,也正是这一切造就了如今的金星,如她所说,"我懂得高处不胜寒的道理,因为我是金星,金星是最亮的一颗星,周边没有其他星星。生命是痛苦的,但过程是美丽的。所以,我把这种生命的痛苦融入肢体语言里,使人们感受到我们共同经历的痛苦。这种痛苦是和美同时存在的,我相信自己行善积德的方式就是,把这种真实的感受,化为生命呈现在舞台上。"     

秋季家常菜如何搭配最营养

<正>人们常常会因快节奏的生活而忽视对日常饮食的要求,很多人仅仅满足于单纯的吃饱就好,忽视了营养的合理搭配。做家常菜要科学搭配,这样既有利于营养,又可诱人食欲,食物搭配合理,会起到营养互补、相辅相成的作用,以下几种饮食搭配可称得上是"鸳鸯配"。1、羊肉配生姜羊肉可补气血和温肾阳,生姜有止痛祛风湿等作用,同时生姜既能去腥膻,又能助羊     

寒旱区盐渍土工程特性研究及展望

介绍寒旱区盐渍土分布的状况及成因,阐述了国内外盐渍土研究和盐渍土病害治理的进展和主要成就,以及近年来西北寒旱地区工程特殊性等领域研究的基本理论、方法和最新进展,探讨了国内对寒旱地区盐渍土岩土工程特性的研究,在此基础上,指出了需要进一步研究的问题.     

野外鉴别石灰岩与白云岩的简易方法以及其对找矿的意义

对于地质工作者来说,鉴别石灰岩和白云岩一直都是个难题。过去所提到的鉴别方法虽然很多,但是都比较麻烦。这里所提到的方法基本上都是用肉眼就能鉴别出来的,熟练掌握此种方法后将大大提高石灰岩和白云岩的鉴别度,并且更加有助于对贮存在石灰岩中的矿床的勘探。此种方法在山东区域内使用均获得了很好的效果。以山东苍山、平邑一带的竹叶石灰岩为例。竹叶石灰岩隶属于寒武系碳酸盐类的沉积岩,它一般由海里的集散碎石,经海水的长时间腐蚀冲击,慢慢形成橄榄状的碎石块,后又经过地壳的运动逐渐被一种钙质胶接、粘合、挤压在一起。